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Plate Tectonics

Plate Tectonics. Earth’s Layers. The crust. Convetion Currents in the Earth's Crust. Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They move like pavement resting on hot tar.

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Plate Tectonics

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  1. Plate Tectonics

  2. Earth’s Layers

  3. The crust Convetion Currents in the Earth's Crust • Lithosphere- rigid, top of the mantle and continents • Asthenosphere- softer and hotter layer underneath • They move like pavement resting on hot tar

  4. The lithosphere looks like a jigsaw puzzle…on the surface of the earth • Tectonic plates- large slabs of rock parts of ocean crust and continents rest on.

  5. Geologists • Geologists study earth processes such as landslides, earthquakes, floods and volcanic eruptions. • Geologists work to understand the history of our planet. The better they can understand Earth’s history the better they can foresee how events and processes of the past might influence the future.  

  6. Alfred Wegener • A geologist who first proposed continental drift theory in 1912 • His hypothesis was that all of earth’s continents were once one giant land mass • Gradually they drifted apart • His scientist peers and friends did not agree until the middle of the 1900’s

  7. Evidence for Continental Drift • 1. Fossil Record: the fossil of the same ancient reptile was found in both South America and southern Africa, but no other place in the world. Both continents must have been joined together at some time in the past.

  8. Evidence for Continental Drift • Evidence of Climate change- • Fossils of ancient ferns from jungles exist on Greenland, which is now covered in ice. Greenland must have once been near the equator. • Evidence of glaciers existed in South Africa, where the climate is now a jungle and desert in parts.

  9. Evidence for Continental Drift • Geology- rock typing found on different continents matches up. Rocks from Brazil matches up with Africa. Carbonado diamonditessupernova rocks that impacted on Earth in the Brazil and Central African Republic area (these were originally next to each other, before the ancient Gondwana continent rifted apart).

  10. Rock Evidence

  11. SuperContinents • Pangaea was formed 270 mya during the Permian and Triassic time periods of Earth’s history. • Most of the dry land was joined together into one huge land mass. • The Permian mass extinction, which wiped out an estimated 96% species about 248 million years ago, was a major event during this time. • Pangaea began to split apart 200 mya http://Pangaea

  12. New Technology, New Discoveries • Scientists began mapping the sea floor • Using drilling, SONAR, lasers bounced off of satellites, and undersea explorers, they started making detailed maps of the sea bed. • These discoveries gave evidence of continental drift and how the tectonic plates moved.

  13. Sea Floor Spreading • Molten rock rises through cracks • It cools and forms new crust • Old crust is pulled away • Oldest crust is pulled down into trenches into asthenosphere and destroyed. CalledSubduction • So…Sea floor is only 180 million years old • Earth continents are 4 billion years old

  14. Sea floor spreads because of…Convection Currents

  15. Sea floor spreading and convection http://Sea Floor Spreading with Bill Nye/ http://earthguide.ucsd.edu/eoc/teachers/t_tectonics/p_paleomag.html

  16. Divergent Boundary • Where plates move apart • Can form Rift Valley on land

  17. Divergent Boundary Example: divergent plate boundary is the Red Sea. Once, the Arabian peninsula and Africa formed a single continent. They are now being ripped apart. The white arrows show the directions the two plates are moving. You can see that a new ocean, the Red Sea is being formed as they separate. 

  18. Convergent Boundary

  19. Convergent Boundary • The dense, leading edge of the oceanic plate actually pulls the rest of the plate into the flowing asthenosphere and a subduction zone is born! Where the two plates intersect, a deep trench forms. • Volcanoes and mountain ranges usually occur along these boundaries. • Think Ring of Fire, Swiss Alps, Appalachian Mountains!

  20. Transform Boundary • Two plates scrape past each other • Usually form along plate lines

  21. Transform Boundary • Example of Transform Boundary would be the San Andreas Fault in California • Earthquakes usually happen along transform boundaries.

  22. Boundaries http://www.classzone.com/books/earth_science/terc/content/visualizations/es0804/es0804page01.cfm?chapter_no=visualization http://www.geo.cornell.edu/eas/education/course/descr/EAS220/2008%20Lectures/Lecture%207%20web/PlateMotionppt.html

  23. Magnetic Reversals http://science.discovery.com/tv-shows/greatest-discoveries/videos/100-greatest-discoveries-magnetic-field-reversal.htm http://Video explanation of sea floor spreading and magnetic reversals

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